出口来自山的冰川养的河流. 梅里,西藏高原的东南部
Tao Pu1, Yanlong Kong2, Shichang Kang1
1Yulong Snow Mountain Cryosphere and Sustainable Development Field Science Observation and Research Station/Key Laboratory of Cryospheric Sciences and Frozen Soil Engineering, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China; State Key Laboratory of Cryospheric Sciences, Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000, China.
Journal of hazardous materials
|July 27, 2024
概括
冰川融水释放 (Hg) 到西藏高原的河流中. 我们的研究表明,明阳河流域充当水槽,Hg出口的季节性变化很大.
科学领域:
- 环境科学 环境科学
- 地质化学 地质化学
- 水文学的水文学
背景情况:
- (Hg) 是一个全球性污染物,在冰层中积累.
- 世界各地的阿尔卑斯山冰川,包括西藏高原 (TP),正在缩小.
- 从冰川融化到河流系统中释放的的研究不足.
研究的目的:
- 量化Hg总度,并从TP的冰川养河出口.
- 调查出口的季节性变化及其与环境因素的关系.
- 为了估计来自整个TP的冰川排水的年度Hg出口量.
主要方法:
- 从2020年10月到2021年10月,每天对明阳河总度的观察.
- 分析Hg度与诸如总悬浮颗粒 (TSP) 和溶解无机碳 (DIC) 等参数之间的相关性.
- 从融水,降水和地下水中计算Hg输入量,以估计出口总量.
主要成果:
- 在季风季节,Hg度比非季风季节更高.
- Hg出口与TSP和DIC度有显著的相关性,有季节性差异.
- 明阳流域被确定为一个Hg沉,总出口量为211.0g (4.3g/km2/年).
结论:
- 在TP的冰川排水对出口做出了重大贡献,估计为947.7公斤/年.
- 季节动态和与TSP和DIC的相关性对于理解Hg运输至关重要.
- 进一步研究冰化水生生态系统中的动力学对于理解循环变化至关重要.
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